Base-level Fluctuation

Base-Level Fluctuation is a geological process denoting oscillations in the elevation of a reference surface that governs the position and movement of sedimentary deposition and erosion boundaries, distinguishing it from static or tectonically driven controls by reflecting changes in the balance between accommodation space and sediment supply in sequence stratigraphy.

28

Publications

1.2K

Citations

76

Authors

48

Institutions

Publications per year

2017–2026

3

Authors

76

  1. AH
    Adrian Harvey

    University of Liverpool, United Kingdom

    2 publications · 112 citations

    2

    h-index

  2. PL
    Paul L. Heller

    University of Wyoming, United States

    1 publications · 114 citations

    1

    h-index

  3. HV
    Helenice Vital

    Universidade Federal do Rio Grande do Norte, Brazil

    1 publications · 27 citations

    1

    h-index

  4. GN
    Gary Nichols

    Royal Holloway University of London, United Kingdom

    1 publications · 24 citations

    1

    h-index

  5. BJ
    Brendan J. Keely

    University of York, United Kingdom

    1 publications · 23 citations

    1

    h-index

1–5 of 76

Venues

  1. Geomorphology

    6 publications · 297 citations

    6

    h-index

  2. Geology

    2 publications · 100 citations

    2

    h-index

  3. Geological Society London Special Publications

    2 publications · 133 citations

    2

    h-index

  4. Sedimentary Geology

    2 publications · 110 citations

    2

    h-index

  5. Marine and Petroleum Geology

    1 publications · 18 citations

    1

    h-index

1–5